Abstract

The author cites the following equation, from Novosolitskii (1965), giving the gravity field due to a slab where the density variation is along the x coordinate only,  
Δg(x)=ρ(s)lnH22+(xs)2H12+(xs)2ds,
(1)
and gives a solution for a special case of linear density variation over a limited zone. Even for such a simple variation, the expression is far too complicated.
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